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ORIGINAL RESEARCH article
Front. Earth Sci.
Sec. Geochemistry
Volume 12 - 2024 |
doi: 10.3389/feart.2024.1454929
Concentration and distribution of B and Se in stream sediments of Zambia and their agricultural implications
Provisionally accepted- 1 Tianjin Center of Geological Survey, China Geological Survey, Tianjin, China
- 2 School of Earth Sciences and Resources, China University of Geosciences, Beijing, Beijing Municipality, China
- 3 Geological Survey Department of Zambia, lusaka, Zambia
- 4 Tianjin Institute of Geological Survey, Tianjin, China
By providing crucial geochemical support for Zambia's foundational geology, agricultural productivity, environmental conservation, mineral exploitation, and other domains, the Sino-Zambian Cooperation project has closed the country's national scale geochemical mapping gap. The overall abundance and geographical distribution of B and Se in Zambian stream sediments are the main objectives of this paper. The median concentrations of B and Se are 12.74 μg/g and 0.056 μg/g, respectively. The distribution patterns of B concentration appeared to be relatively uniform, lacking distinct indicators, whereas that of Se was more pronounced. In comparison to other tectonic belts, the Domes Region, Lufilian Arc and Choma-Kalomo Block have greater median and average concentrations of Se. Black shales and vast epithermal metallogenic zones are common in the Kawana-Solwezi-Ndola and the Mansa-Mporokoso-Kasama regions, which also have high Se contents. These regions could serve as promising places for the advancement of selenium-enriched agricultural practices.
Keywords: Catchment sediment, Geochemical mapping, Soil of cultivated land, Agricultural applications, Zambia H. Sun, No. 4, The 8th Road, Dazhigu, Hedong District,
Received: 04 Jul 2024; Accepted: 17 Dec 2024.
Copyright: © 2024 Sun, Ren, Wang, Zuo, He, Wu, Xu, Mukofu, Dokowe and Cao. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
* Correspondence:
Hongwei Sun, Tianjin Center of Geological Survey, China Geological Survey, Tianjin, China
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